Majorite is a high-pressure garnet variety typically found as microscopic inclusions within diamonds or as a product of meteorite impacts. It is characterized by its high-pressure structure and is highly sought after by mineralogists studying deep mantle processes.
Is this majorite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch majorite with a known reference. Majorite sits at Mohs 7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Majorite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Majorite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: purple, violet, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: equant grains, inclusions in diamonds.
Often confused with
Majorite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside majorite
Minerals reported to co-occur with majorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃(Fe,Si,Al)₂(SiO₄)₃
- Mohs hardness
- 7.5
- Density
- 3.5-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Equant Grains, Inclusions in Diamonds
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Mantle-derived Xenoliths, Kimberlites, Meteorite Impact Sites
- Typical price
- $100-500 per micro-mount or diamond inclusion sample
Where rockhounds find majorite
Classic worldwide localities
- Coorara meteorite, Australia
- Kokchetav Massif, Kazakhstan
- various diamond-bearing kimberlite pipes
Field-hunting tip
Look in mantle-derived xenoliths, kimberlites, meteorite impact sites country — that is the host setting where majorite typically forms. If you start seeing diamond, enstatite, omphacite in float, you are in the right ground. Field specimens usually show a equant grains, inclusions in diamonds habit, so train your eye for that shape before scanning the outcrop.




